Haverhill Water Hardness & Quality Report (2026)
Water Hardness
15.3°Clark21.8°fH12.2°dH
Source
mixed
pH Level
7.9
neutral = 7.0
Lead
0.002 mg/L
✓ Below action level
TDS
516.1 mg/L
Est. Daily Cost
£0.49
energy & soap waste
Source: DWI Data Portal · Updated 2026
0–60
mg/L
Soft
61–120
mg/L
Moderately Hard
121–180
mg/L
Hard
180+
mg/L
Very Hard
Appliance Damage Report
In Haverhill, your appliances are currently losing 29% efficiency due to mineral buildup.
| Appliance | In Haverhill | Soft Water City | Efficiency Loss |
|---|---|---|---|
| Kettle | 2.4 yrs | 8.5 yrs | -72% |
| Washing Machine | 5.5 yrs | 12 yrs | -54% |
| Water Heater | 6.9 yrs | 15 yrs | -54% |
Regional Water Comparison
How Haverhill compares to its nearest neighbours
| City | Hardness | Clark° | Risk | Source |
|---|---|---|---|---|
| ▶ Haverhill, East of England | 218 mg/L | 15.3° | 🔴 Very Hard | mixed |
| Newmarket, East of England | 183 mg/L | 12.8° | 🔴 Very Hard | mixed |
| Saffron Walden, East of England | 317.5 mg/L | 22.3° | 🔴 Very Hard | mixed |
| Braintree, East of England | 221.5 mg/L | 15.5° | 🔴 Very Hard | mixed |
| Halstead, East of England | 244.5 mg/L | 17.2° | 🔴 Very Hard | mixed |
National Benchmark
How Haverhill compares to the United Kingdom average
| Benchmark | Hardness | Appliance Risk |
|---|---|---|
| ▶ Haverhill | 218 mg/L | 🔴 High |
| United Kingdom National Avg | 183 mg/L | 🔴 High |
| Livingston Top Rated | 8.5 mg/L | 🟢 None |
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What Makes Haverhill's Water Unique?
Local geology and source profile
Haverhill, the south-west Suffolk town on the Essex border in the upper Stour valley, is served by Essex & Suffolk Water. Supply to south-west Suffolk and the Haverhill area draws on two complementary sources: chalk groundwater from the Suffolk Chalk Aquifer — boreholes in the chalk dip slope of south Suffolk and the west Essex chalk country — and surface water abstracted from the River Stour treated at Alpheton Water Treatment Works near Long Melford. The River Stour drains the Suffolk and Essex chalk uplands, carrying dissolved calcium bicarbonate from its chalk catchment. The blend of chalk borehole water and chalk-fed river water produces consistently hard water at 218 mg/L in the Haverhill distribution zone. The TDS of 516.1 mg/L reflects chalk carbonate groundwater with modest additional sulphate and sodium from deeper chalk horizons and glacial drift overlying the aquifer.
The Cretaceous Chalk forms the bedrock beneath the gentle rolling arable landscape of south-west Suffolk and west Essex. Groundwater in the unconfined chalk at depths of 30–60 m acquires calcium bicarbonate concentrations of 200–230 mg/L from the chalk matrix over residence periods of months to a few years. The River Stour headwaters above Haverhill drain the same chalk country, reinforcing the hard-water character of the surface-water supply fraction. East Anglia is defined by its chalk geology, and Haverhill exemplifies the consistently hard water characteristic of the south Suffolk chalk belt.
At 218 mg/L Haverhill's water is hard and limescale is a persistent household presence. Kettles should be descaled monthly using a citric acid tablet or white vinegar. Shower screens and tile grout accumulate calcium deposits that benefit from weekly cleaning with a limescale spray. Washing-up liquid must be used generously. Combi-boilers and washing machines benefit from inline scale inhibitors. In Haverhill's growing town housing stock — including many 1960s–1980s new-build estates — consistent appliance maintenance is essential to maintain heating system efficiency and avoid costly repairs from hard Suffolk chalk water.
Geology & Source: Supplied by Essex & Suffolk Water from the Suffolk Chalk Aquifer and Stour valley surface water — East Anglian chalk groundwater blend with River Stour abstraction — produces hard water at 218 mg/L (15.3°Clark).